Sandstone can be transformed into sediment if lithificaton dues not occur.
No. Sandstone is sedimentary rock, where the individual grains of sand that compose the rock are visible without magnification. These individual grains of sand (sediment) have become compacted and cemented together in a process called lithification, forming a sedimentary rock.Metamorphic rock can be formed from virtually any parent rock (protolith) that has been subjected to heat and/or pressure, modifying its texture or mineral composition.Quartz sandstone, when metamorphosed, becomes the metamorphic rock 'quartzite'.
Sedimentary rocks such as sandstone, shale, and limestone can weather and wear away to form sediment. These rocks are often composed of loose grains that can be eroded by wind, water, or ice, leading to the formation of sediment.
Sandstone typically has uneven layers due to varying amounts of pressure and sediment accumulation during formation. This creates a distinct, layered appearance in the rock.
The type of rock made of hardened sediment is called sedimentary rock. Sedimentary rocks are formed through the accumulation and compression of sediments such as sand, silt, and clay over time. Examples of sedimentary rocks include sandstone, shale, and limestone.
Rocks formed from sediment deposits are called sedimentary rocks. They are formed from the accumulation and lithification of sediment, which can include fragments of pre-existing rocks, minerals, and organic material. Examples include sandstone, shale, and limestone.
a deposit can change laterally, so it might be deposited a conglomerate upstream and further downstream a sandstone, but once it is deposited it cannot be transformed unless it is subject to heat and/or pressure, it will then be a metamorphic rock. If the river is in retrograde then the deposit will grade upwards from a conglomerate to a sandstone
No. Sandstone is sedimentary rock, where the individual grains of sand that compose the rock are visible without magnification. These individual grains of sand (sediment) have become compacted and cemented together in a process called lithification, forming a sedimentary rock.Metamorphic rock can be formed from virtually any parent rock (protolith) that has been subjected to heat and/or pressure, modifying its texture or mineral composition.Quartz sandstone, when metamorphosed, becomes the metamorphic rock 'quartzite'.
Sedimentary rocks such as sandstone, shale, and limestone can weather and wear away to form sediment. These rocks are often composed of loose grains that can be eroded by wind, water, or ice, leading to the formation of sediment.
one of them is sandstone.
sandstone
Sandstone typically has uneven layers due to varying amounts of pressure and sediment accumulation during formation. This creates a distinct, layered appearance in the rock.
The forces of the mountain building slowly pushed the granite upward. This formed a mountain. Water and wind slowly wore the granite away. The sand remaining was carried by streams to the ocean. Over millions of years layers of sediment piled up on the ocean floor and changed to sandstone. Sandstone is a Sedimentary rock. Over time, the sandstone became deeply buried. Heat and pressure changed the sandstone to quartzite, a metamorphic rock. I got this from my science homework. :)
Erosion. If a metamorphic rock is exposed above sea level it will erode or weather, the products from this erosion or weathering will be moved by gravity, wind or water to a sea or basin where the products will settle as a sediment. If the conditions are right the sediment will eventually become a sedimentary rock.
the granite melts into lava then cools becoming igneous. it erodes into sediment and then gets compressed into a sedimentary rock. the sedimentary rock becomes metamorphic with heat and pressure deep within Earth
Granite becomes Sandstone when water erodes the Granite on Earths surface, and then deposits the sediment.
By exposure to heat and/or pressure through depth of burial, directed pressure, or proximity to a magma source. Existing minerals can recrystallize, non-hydrous minerals can replace hydrous minerals, new minerals can be formed from the introduction of new ions from heated solutions, and minerals can become flattened and aligned in parallel layers.
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